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Introduction to the resistivity surveying method. The resistivity of ...

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function basically tells us <strong>the</strong> degree <strong>to</strong> which a change in <strong>the</strong> <strong>resistivity</strong> <strong>of</strong> a section <strong>of</strong> <strong>the</strong><br />

subsurface will influence <strong>the</strong> potential measured by <strong>the</strong> array. <strong>The</strong> higher <strong>the</strong> value <strong>of</strong> <strong>the</strong><br />

sensitivity function, <strong>the</strong> greater is <strong>the</strong> influence <strong>of</strong> <strong>the</strong> subsurface region on <strong>the</strong> measurement.<br />

Note that for all <strong>the</strong> three arrays, <strong>the</strong> highest sensitivity values are found near <strong>the</strong> electrodes.<br />

At larger distances from <strong>the</strong> electrodes, <strong>the</strong> con<strong>to</strong>ur patterns are different for <strong>the</strong> different<br />

arrays. <strong>The</strong> difference in <strong>the</strong> con<strong>to</strong>ur pattern in <strong>the</strong> sensitivity function plot helps <strong>to</strong> explain<br />

<strong>the</strong> response <strong>of</strong> <strong>the</strong> different arrays <strong>to</strong> different types <strong>of</strong> structures.<br />

Table 2 gives <strong>the</strong> median depth <strong>of</strong> investigation for <strong>the</strong> different arrays. <strong>The</strong> median<br />

depth <strong>of</strong> investigation gives an idea <strong>of</strong> <strong>the</strong> depth <strong>to</strong> which we can map with a particular array.<br />

<strong>The</strong> median depth values are determined by integrating <strong>the</strong> sensitivity function with depth.<br />

Please refer <strong>to</strong> <strong>the</strong> paper by Edwards (1977) listed in <strong>the</strong> Reference section for <strong>the</strong> details. In<br />

layman's terms, <strong>the</strong> upper section <strong>of</strong> <strong>the</strong> earth above <strong>the</strong> "median depth <strong>of</strong> investigation" has<br />

<strong>the</strong> same influence on <strong>the</strong> measured potential as <strong>the</strong> lower section. This tells us roughly how<br />

deep we can see with an array. This depth does not depend on <strong>the</strong> measured apparent<br />

<strong>resistivity</strong> or <strong>the</strong> <strong>resistivity</strong> <strong>of</strong> <strong>the</strong> homogeneous earth model. It should be noted that <strong>the</strong><br />

depths are strictly only valid for a homogeneous earth model, but <strong>the</strong>y are probably good<br />

enough for planning field surveys. If <strong>the</strong>re are large <strong>resistivity</strong> contrasts near <strong>the</strong> surface, <strong>the</strong><br />

actual depth <strong>of</strong> investigation could be somewhat different. For example, it has been observed<br />

that a large low <strong>resistivity</strong> body near <strong>the</strong> surface tends <strong>to</strong> create a “shadow zone” below it<br />

where it is more difficult <strong>to</strong> accurately determine <strong>the</strong> <strong>resistivity</strong> values.<br />

To determine <strong>the</strong> maximum depth mapped by a particular survey, multiply <strong>the</strong><br />

maximum “a” electrode spacing, or maximum array length “L“, by <strong>the</strong> appropriate depth<br />

fac<strong>to</strong>r given in Table 2. For example, if <strong>the</strong> maximum electrode “a” spacing used by <strong>the</strong><br />

Wenner array is 100 metres (or maximum L 300 metres), <strong>the</strong>n <strong>the</strong> maximum depth mapped is<br />

about 51 metres. For <strong>the</strong> dipole-dipole, pole-dipole and Wenner-Schlumberger arrays, ano<strong>the</strong>r<br />

fac<strong>to</strong>r “n” must also be taken in<strong>to</strong> consideration. For <strong>the</strong> arrays with four active electrodes<br />

(such as <strong>the</strong> dipole-dipole, Wenner and Wenner-Schlumberger arrays), it is probably easier <strong>to</strong><br />

use <strong>the</strong> <strong>to</strong>tal array length “L”. As an example, if a dipole-dipole survey uses a maximum<br />

value <strong>of</strong> 10 metres for “a” and a corresponding maximum value <strong>of</strong> 6 for n, <strong>the</strong>n <strong>the</strong> maximum<br />

“L” value is 80 metres. This gives a maximum depth <strong>of</strong> investigation <strong>of</strong> 80x0.216 or about 17<br />

metres.<br />

Table 2 also includes <strong>the</strong> geometric fac<strong>to</strong>r for <strong>the</strong> various arrays for an "a" spacing <strong>of</strong><br />

1.0 metre. <strong>The</strong> inverse <strong>of</strong> <strong>the</strong> geometric fac<strong>to</strong>r gives an indication <strong>of</strong> <strong>the</strong> voltage that would be<br />

measured between <strong>the</strong> P1 and P2 potential electrodes. <strong>The</strong> ratio <strong>of</strong> this potential compared <strong>to</strong><br />

<strong>the</strong> Wenner alpha array is also given, for example a value <strong>of</strong> 0.01 means that <strong>the</strong> potential is<br />

1% <strong>of</strong> <strong>the</strong> potential measured by <strong>the</strong> Wenner alpha array with <strong>the</strong> same "a" spacing.<br />

2.5.1 Wenner array<br />

This is a robust array that was popularized by <strong>the</strong> pioneering work carried by <strong>The</strong><br />

University <strong>of</strong> Birmingham research group (Griffiths and Turnbull 1985; Griffiths, Turnbull<br />

and Olayinka 1990). Many <strong>of</strong> <strong>the</strong> early 2-D surveys were carried out with this array. In Figure<br />

8a, <strong>the</strong> sensitivity plot for <strong>the</strong> Wenner array has almost horizontal con<strong>to</strong>urs beneath <strong>the</strong> centre<br />

<strong>of</strong> <strong>the</strong> array. Because <strong>of</strong> this property, <strong>the</strong> Wenner array is relatively sensitive <strong>to</strong> vertical<br />

changes in <strong>the</strong> subsurface <strong>resistivity</strong> below <strong>the</strong> centre <strong>of</strong> <strong>the</strong> array. However, it is less<br />

sensitive <strong>to</strong> horizontal changes in <strong>the</strong> subsurface <strong>resistivity</strong>. In general, <strong>the</strong> Wenner is good in<br />

resolving vertical changes (i.e. horizontal structures), but relatively poor in detecting<br />

horizontal changes (i.e. narrow vertical structures). In Table 2, we see that for <strong>the</strong> Wenner<br />

array, <strong>the</strong> median depth <strong>of</strong> investigation is approximately 0.5 times <strong>the</strong> “a” spacing used.<br />

Compared <strong>to</strong> o<strong>the</strong>r arrays, <strong>the</strong> Wenner array has a moderate depth <strong>of</strong> investigation. <strong>The</strong> signal<br />

Copyright (1999-2001) M.H.Loke

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